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1)  continuous medium
连续介质
1.
In the first step,through using the formula of the conformal transformation,a continuous medium with regulation boundary in original area could be transformed to a homogeneous medium with anomalous boundary in complex area,so the new constant velocity field could be more adapt to the current Stolt migration's conditions.
首先,利用保角变换法可将不规则边界的单连通区域转变成规则边界的原理,将规则边界的连续介质场转变成不规则边界的均匀介质场,使该均匀介质场更适应现有Stolt等偏移方法对速度场的要求;其次,对改变了区域的模型地震记录进行常规的偏移成像处理;再利用推导出的反变换公式对成像结果进行反变换,得出模型的真实偏移成像结果。
2.
In macro-scale of time and space,the dispersed cuttings phase is assumed to behave as continuous medium,which is termed "pseudo-fluid", and its dynamic regularity is shown in the view of statistics.
但是,在时间与空间的宏观尺度下,其分布及运动又具有统计连续性与规律性,并可将其视为一种特殊的连续介质──拟流体。
3.
By using the law of reflection,the equation of time distance curve of reflection wave under the continuous medium tilted interface,is discussed.
应用反射定律,讨论了连续介质斜界面下的反射波时距曲线方程,给出了这类模型下的成像方
2)  continuum [英][kən'tɪnjuəm]  [美][kən'tɪnjuəm]
连续介质
1.
Verification of the Drawing Theory in the Continuum (Ⅰ);
连续介质放矿理论的检验(上)
2.
Verification of The Drawing Theory in the Continuum (Ⅱ);
连续介质放矿理论的检验(下)
3.
Discussion on Seepage through Continuum and Seepage through Non-continuum;
连续介质渗流与非连续介质渗流
3)  continuous media
连续介质
1.
Universal dynamics equation in continuous media was deduced using tensor.
利用张量记号推导出连续介质动力学普遍方程式 ,并由此得到弹性力学的Navier方程和理想流体动力学的Euler方
2.
While wells are producing, heat transfer in welibore is considered as heat conduction and convection in continuous media in vertical tube, heat transfer in production zones is considered as heat conduction and convection in porous media, heat transfer in adjacent rocks is considered as heat conduction in porous medi.
当油井生产时,将井筒内传热看成竖直圆管中连续介质的传导和对流换热,将地层中产层部分的传热看成多孔介质中的传导和对流换热,将地层中围岩部分的传热看成多孔介质中的热传导;当油井停产时,由于井筒和产层都没有了流体的流动,所以将井筒内的传热看成竖直圆管中连续介质的传导,将地层中的传热看成多孔介质中的传导。
4)  discontinuous medium
不连续介质
1.
Reinforcement and concrete bear loads together by bonding on their interfaces,and interface stress is a discontinuous medium-related mechanical problem.
钢筋与混凝土主要通过界面黏结作用来共同承受荷载,在界面上的受力属于不连续介质的力学问题。
2.
The stochastic interface stress element method for solving the reliability of continuous or discontinuous medium structures is introduced for the first time.
首次提出适用于求解连续及不连续介质结构可靠度的随机界面元法,建立了数学模型,导出了基本公式,研制了计算程序。
5)  Cosserat continua
Cosserat连续介质
1.
Classical yield criterions cannot be applied directly to Cosserat continua since the strain tensor and stress tensor in Cosserat continua are asymmetric.
Cosserat连续介质下的应力、应变张量具有不对称性,经典连续介质的屈服准则无法直接用于 Cosserat连续介质
6)  block fractured medium
拟连续介质
1.
Considering the characteristics of rockmass,a 3D coupled seepage model of jointed rock mass and its FEM program are developed, which is based on the conception of equivalent continuum and block fractured medium.
根据岩体实际性态,提出了基于块裂介质和拟连续介质的裂隙岩体三维渗流耦合数学模型,并编制了三维有限元程序。
补充资料:连续介质
连续介质
continuum

   流体力学或固体力学研究的基本假设之一。它认为流体或固体质点在空间是连续而无空隙地分布的,且质点具有宏观物理量如质量、速度、压强、温度等,都是空间和时间的连续函数,满足一定的物理定律(如质量守恒定律、牛顿运动定律、能量守恒定律、热力学定律等)。所谓质点,实际是指微观充分大、宏观充分小的分子团,也称微团。即其尺度比分子或分子运动尺度足够大,它可以包含“无数”的分子,而比所研究力学问题的特征尺度足够小。有了连续介质假设,就可以在流体力学研究中广泛运用数学分析这一强有力的工具。实际流体的结构在一般情况下是非常接近连续介质模型的  。例如在冰点温度(273.15开)和标准大气压(101325帕)下,1立方厘米空气含分子约2.7×1019个,分子平均自由程约10-9厘米(液体比气体更为“致密”),1秒内分子碰撞约1029次。显然,从力学角度完全可以忽略分子结构的离散性和分子碰撞作用的间歇性,而认为物质是连续的。在特殊情况,如稀薄气体中,分子自由程相比力学特征尺度已不是非常小,因而连续介质假设不适用;激波层的厚度为分子量级,研究激波层中的气体运动也不能用连续介质假设。
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